These pages have been constructed in fulfillment of the
final project assignment for GEOS.5405 (Remote Sensing) at the University
of Texas at Dallas for the fall term 2000.
Petrologic Analysis of Eastern Sultanate of Oman
by Leslie F. Bleamaster III
Introduction
The
Sultanate of Oman is host to the Earth's largest mass of exposed ancient
oceanic crust, the Samail Ophiolite. Rock types within the ophiolite
include peridiotites, gabbros, basalts, and serpentanites. The surrounding
geology is a complex collection of intensely deformed quartzites, mafic
schists (including eclogite assemblages), calc-schists, dolomites and other
carbonates. Because of Oman's dry climate, lack of vegetation, and
minimal cloud cover, studying the Samail Ophiolite and the surrounding
area by remote sensing means is facilitated. Three remote data sets,
1) LANDSAT (5) TM [scenes 159-44 and 158-43], 2) CORONA satellite photography
[scenes DS09059A008MC028 and DS09034A023MC055], and 3) a G-topo digital
elevation model (DEM), were originally proposed to be the primary, secondary,
and tertiary data sets, respectfully, however, only the LANDSAT and DEM
data sets proved to be useful. Geologic mapping was based primarily
on the interpretation of the two LANDSAT scenes, whereas the DEM provided
a spatial context, and facilitated visualization of the ground terrain.
The DEM provided no major geologic contributions, but it did make for some
very nice images.
As proposed, the results of this work were compared with
the field mapping completed by Gregory, R.T., Gray, D.R., and Miller, J.M.,
near Masqat, Oman. The mapping completed within this project has
no where near the lithologic or structural detail achieved by the ground
team, however, geologic units discerned from the remote data do correlate
well with those of Gregory, Gray, and Miller. Preliminary evaluation
has raised some interesting questions and further investigation of the
remote data may provide reconnaissance maps for future field studies northwest
of Masqat.
Ophiolites
The term ophiolite refers to a distinctive rock assemblage
containing ultramafic, gabbroic, and basaltic rocks, which are commonly
capped by a thin veneer of deep-sea pelagic sediments. The emplacement
of ophiolites is still not well understood but certainly seems to be the
result of convergence between oceanic and continental plates. In
the simplest and most straight forward model, the beginning of subduction
at a newly activated old passive margin results initially in some of the
ocean plate overriding the edge of the continental plate before normal
subduction of oceanic lithosphere can be established. This process,
called obduction, overthrusts oceanic crust onto the continental margin
and results in a cross sectional display of the uppermost layers of the
oceanic crust. This simple model does not particularly explain the
processes which occured in Oman, but never the less, the ophiolite does
represent ancient oceanic crust and the use of the LANDSAT 5 false color
images do provide the ability to produce a simplified geologic map and
statigraphic sequence for the region without ever leaving the comfort of
the air conditioned lab.
Data
LANDSAT 5 scenes, received from Robert Gregory, were used
as my primary data set. The use of the software program ENVI, available
through the UT
Dallas Remote Sensing Laboratory, allowed manipulation of the spectral
data. True color (3-2-1, Figure 1) images,
as well as band ratio images [i.e. Sultan's combination (5/7-5/1-3/4*5/4,
Figure
2), and Abrahmís combination (5/7-4/5-3/1, Figure
3)], were all helpful in distinguishing major geologic units, however
Sultan's combination (Figure2) proved to be the
most valuable for differentiating lithologic differences both within and
surrounding the ophiolite.
As a secondary data source I used a G-topo digital elevation
model made available through the UTD Laboratory. The DEM's spatial
resolution footprint is approximately 800 meters which is much coarser
than the LANDSAT's 30 meter resolution. By generating a topo-map
with 200 ft contours, it can be easily seen that the ophiolite and associated
carbonate units are high standing and make up the bulk of the Oman montains
that arch from the southeast to the northwest parrallelling the coastline.
The topography data also shows the two structural windows though which
the basement rocks are exposed. Although the limited resolution of
the DEM does not allow for direct evaluation of topographic/lithologic
relationships it can be used to enhance the LANDSAT 5 images by providing
a three-dimentional spatial context. Draping the Sultan's combination
images over the DEM does show a broad corelation of lithology to topography
(Figure 4). The DEM was also used to create
a 360 degree fly around above the southeastern (158-44) true color LANDSAT
image (Figure 5).
Of the two mosaic CORONA scenes purchased from the USGS,
only one was scanned and evaluated. The smallness of the hard copy
image (5 x 5 inches) proved to be too small to provide adequate resolution,
even when scanned at the highest resolution possible. Perhaps individual
CORONA swaths, rather than mosaics would provide better resolution images.
Although the image was not used during this petrologic analysis, I am making
the image available here at greatly reduced resolution (DS09034A023MC055)
for you viewing.
Remote data/ Field Mapping Comparison
Using the map of the Saih Hatat by Gregory, Gray, and
Miller as a guide to interpret the different colors produced by stretching
the LANDSAT images (Figure 6), lithologic relationships
were extended into other portions of the ophiolite to produce a simplified
geologic
map showing some of the large scale lithologic units and structural
relationships. More detailed studies are to come. Please stay
tuned.
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